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Sea level change

dc.contributor.authorChurch, J.A.
dc.contributor.authorClark, P.U.
dc.contributor.authorCazenave, A.
dc.contributor.authorGregory, J.M.
dc.contributor.authorJevrejeva, S.
dc.contributor.authorLevermann, A.
dc.contributor.authorMerrifield, M.A.
dc.contributor.authorMilne, G.A.
dc.contributor.authorNerem, R.S.
dc.contributor.authorNunn, P.D.
dc.contributor.authorPayne, A.J.
dc.contributor.authorPfeffer, W.T.
dc.contributor.authorStammer, D.
dc.contributor.authorUnnikrishnan, A.S.
dc.date.accessioned2014-09-19T09:56:49Z
dc.date.available2014-09-19T09:56:49Z
dc.date.issued2013
dc.identifier.citationClimate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. ed. by: Stocker, T.F.; Qin, D.; Plattner, G.-K.; Tignor, M.; Allen, S.K.; Boschung, J.; Nauels, A.; Xia, Y.; Bex, V.; Midgley, P.M.; Cambridge; UK; 2013; 1137-1216.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/4605
dc.description.abstractThis chapter considers changes in global mean sea level, regional sea level, sea level extremes, and waves. Confidence in projections of global mean sea level rise has increased since the Fourth Assessment Report (AR4) because of the improved physical understanding of the components of sea level, the improved agreement of process-based models with observations, and the inclusion of ice-sheet dynamical changes.
dc.language.isoen
dc.publisherP.M.Cambridge University Press
dc.rights© Intergovernmental Panel on Climate Change 2013.
dc.subjectsea level changes
dc.subjectsea level measurement
dc.subjectflooding
dc.subjectcoastal morphology
dc.subjectprediction
dc.subjectlong-term changes
dc.subjectpalaeoshorelines
dc.titleSea level change
dc.typeTechnical Report


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